AN ASSESSMENT REPORT ON
THE GEOLOGY AND GOLD POTENTIAL OF THE LINDA 1-5, BEAN AND BANJO 3 CLAIMS
NTS 103 F/9 Latitude 53O35'N Longitude 132O23'W
OWNED AND OPERATED BY
Vancouver, British Columbia V6C 2x8
BY
TABLE OF CONTENTS
3.1 3.2 3.3 3.4 3.5 3.5.1 3.5.2 3.5.3 3.5.4 3.5.5
5 5 5 8 9 9 9 9
10 10
............................... ........................ .................
............................. ................................ ................................
ACKNOWLEDGEMENTS...............................
MAPS AND FIGURES
3
1.0 RECOMMENDATIONS
Mapping and extensive sampling has failed to uncover any areas of potential interest within the Linda 1-5 Claims, Banjo 3 and the Bean Claim.
No further work is recommended within the claims.
4
2.0 SUMMARY AND CONCLUSIONS
1. The property is underlain by the Masset Formation, a suite of volcanic rocks ranging in composition from basalt to rhyolite. Minor sedimentary units are intercalated within the volcanic rocks.
2. Brecciation and alteration in the rhyolites was previously attributed to hydrothermal alteration. More detailed investigation has shown that the brecciation occurs in the basal and upper portions of the rhyolites and that it occurred contemporaneously with extrusion and emplacement of the flow. Similarly, the extensive clay alteration (seritization of feldspars) noted in these rocks was most probably caused by gas devolitization and cooling during emplacement of the flows.
3 . Extensive sampling has returned isolated anomalous values in mercury, arsenic and gold. Investigations have failed to locate the source(s) of these isolated anomalies within the claim boundaries. However, it is felt that such mineralization is most likely associated with faulting .
5
3.0
3.1
INTRODUCTION
PROPERTY DESCRIPTION
The Linda 1-5 Claims consisting of 79 units are located to the east of Juskatla Inlet between Towustasin Hill and Blackwater Creek to the south (Fig. 1). More specifically, the claims are centred about latitude 53O35'N and longitude 132O23'W on NTS map sheet 103F/9 on the Queen Charlotte Islands (Fig. 2). The claims are owned and operated by City Resources (Canada) Limited, #2000-666 Burrard Street, Vancouver, British Columbia, V6C 2x8.
The Bean Claim, situated between Linda 1 and Linda 5
Claims, was staked by its present owner, Roy Woolverton in 1978 and was previously optioned to New Pioneer Explorations. The Bean Claim is presently under option to City Resources (Canada) Limited.
3.2 ACCESS
The claims group can be reached by turning southwest at the Juskatla Inlet logging camp and following the Datlamen Main for approximately 8 km and then taking the Towustasin Main into the Bird and Collinson Lake area. Once on the claim group, numerous logging roads and spur roads provide excellent access to most of the ground covered by the claims.
3.3 CLAIM DESCRIPTION
Total
Assessmen
3.4 FIELD METHODS
The field work described in this report was carried out by the author from June 21 to July 25, 1988.
Outcrop was mapped at all locations encountered and notations on structure, mineralization and alteration were recorded. The results are shown on Maps 1-5 in the pocket at the back of this report. These 1:5,000 scale maps were prepared from base maps provided by MacMillan Bloedel Limited.
All mineralized outcrop was systematically sampled by taking either grab samples or representative chip samples. In addition, the larger streams were panned and a pan concentrate sample was collected for analysis. A silt sample was also taken at this site. Soil samples were taken across slopes in areas of interest.
Much of the timber cover on the claims has been removed by clear cut logging and outcroppings that would not have been visible beforehand are now clearly exposed. However, dense secondary growth and abandoned timber greatly impede access to these outcrops.
9
3.5 GEOCHEMICAL SAMPLING
A total of 159 samples consisting of 21 silts, 51 rocks, 68 soils and 13 panned concentrates were collected.
These samples were sent to Chemex Labs Ltd in North Vancouver for analysis. Their analytical method is given below.
3.5.1 Sample Preparation
Soil and silt samples are sorted, dried at 40.5OC, screened to -80 mesh; rock samples are sorted, crushed, split in a Jones riffler; pulverized in a ring pulverizer.
3.5.2 Analyses
To analyze for Ag, Pb, Zn, Cu and Mo, a one gram sample is decomposed for two hours in a perchloric acid and nitric acid mixture, cooled, diluted to volume and analyzed on an AA5 spectrophotometer. Detection limits are 0.1 ppm for silver and 1.0 ppm for base metals. Gold analyses begins with a 10 gm sample which is mixed with litharge (PbO) sodium carbonate, silica, borax glass, flour and 10 mg of silver; this mixture is fused in a fire assay furnace, the melt poured into steel moulds and the resulting button containing gold and silver is cupelled, leaving a dore' bead which is dissolved in acids, diluted in HC1 and analyzed to a detection limit of 5 ppb for gold on an AA5 spectrophotometer.
3.5.3
Soil samples from the lower "8" horizon were collected throughout the claims group with an emphasis on drainage basins recommended for follow up on previous exploration programs. Care
10
was taken to collect samples below the organic or "A" horizon which varied in thickness from a few cm to in excess of 20 cm.
Ten soil samples returned values of between 5 and 20 ppb Au. These isolated samples were not anomalous in other elements and are not considered to warrant further follow up.
3.5.4 Pan Concentrates
Heavy mineral pan concentrates were collected from all major streams and significant tributaries on the claims group. Samples were generally obtained from sieving moss taken from boulders in the stream, where moss was not present, or when the moss did not contain sufficeint sediment, samples were concentrated from gravels in the stream.
No pan concentrates returned values considered to be anomalous in gold or related elements.
3.5.5 Rocks
Rock samples were obtained primarily from fresh outcrop surf aces.
Emphasis was placed on mineralized outcrop and those rocks which had the appearance of secondary silicification or other alteration.
Eight rocks returned weekly anomalous values in gold and several were weakly to moderately anomalous in mercury.
11
4 . 0 GENERAL GEOLOGY
The claims are underlain by the Tertiary Masset Formation consisting of interbedded basalts, rhyolitic to dacitic pyroclastics and rhyolite flows intruded by minor andesitic to basaltic dykes. Minor sedimentary units consisting of primary volcanic debris (lahars) and reworked volcanic material are also encountered on the property. The area is cut by numerous fractures and faults that are typically high angle and have a north easterly trend. The Masset volcanics are commonly aphanitic and lack phenocrysts (aphyricl. Weathered surfaces range in colour from buff through grey to black and in general conform to the mixed unit of the Tartu Inlet facies of the Masset Formation as described by Sutherland-Brown (1968).
4.1 LITHOLOGY
In order to simplify mapping, the rocks were divided into three basic units: felsic rocks, mafic rocks and sedimentary rocks. The felsic rocks are all aphanitic and further classifications was based primarily on phenocryst type as follows; aphanitic aphyric (no phenocrysts visible), feldspar phyric and quartz-felspar phyric. Mafic rocks were subdivided into aphanitjc aphyric and aphanitic with feldspar and pyroxene phenocrysts. On occasion, eguigranular "sugary" textured basalts were encountered. Sedimentary rocks are either primary volcanic deposits emplaced by sedimentary processes or reworked volcanic material.
Pollen age determinations and K argon dates give a time span of early to mid Miocene to early Pliocene for the emplacement of Masset volcanics in the vicinity of the claims group (C. J. Hickson 1988 and 1989).
12
The basal section of the sequence is made up of a thick sequence of mafic flows (individual flows up to 30 m) which are associated with interflow breccias.
This basal sequence is conformably overlain by a mixture of dacitic to rhyolite pyroclastic flows and lava flows with minor interfingering mafic lava flows.
Rhyolite pyroclastic and flow rocks predominate above the mixed sequence. Unconformably overlying this sequence is a thick unit of volcanoclastic sediments which forms Towustasin Hill and upper portions of Juskatla Mountain. Localized valley filling intermediate to basalt composition flows mark the last eruptive event in this sequence.
Interflow sediments are minimal and there is little evidence of erosion between eruptive events.
4.2 STRUCTURE
In general, faults and shears on the property are high angle and range between Oo-50° dipping steeply northwest and 15Oo-18O0 dipping steeply to the northeast. In most cases offset along the faults is minimal. On the Blackwater Creek side of Juskatla Mountain, a series of northtrending en echelon faults were observed with an aggregate offset of about 10 m.
4.3 ALTERATION AND MINERALIZATION
Extensive clay alteration accompanied by silicification and brecciation in the rhyolites has previously been attributed to hydrothermal alteration. However, discussions with C . J. Hickson, Geological Survey of Canada and detailed investigation
13
in the field show that; (i) the clay alteration is caused by gas devolitization and cooling during emplacement of the flows, (ii) brecciation occurs in the basal and upper portions of the rhyolite flows and similarly occurs during emplacement, (iii) the rhyolite contains up to 76% silica ( C . J. Hickson 1988) thus accounting for the strongly silicified appearance of these rocks.
4.3.2 MINERALIZATION
Pyrite and arsenopyrite were the only sulphides encountered. Pyrite commonly and arsenopyrite less commonly occur in the basal and flow top breccias in the rhyolites, in faults (where pyrite forms 8-10 cm clumps and masses in the clays) and in narrow (1-2 cm) quartz veins.
Disseminated pyrite is also common in the dykes and mafic flows. None of this mineralization was found to have any economic significance.
4.4 GEOCHEMICAL RESULTS
Results from geochemical sampling are not encouraging and have failed to identify any areas of potential interest. No anomalous gold values were found in rock, silt or soil samples. One anomalous pan concentrate sample was collected, however other samples upstream failed to return anomalous values.
Several rock samples from narrow sheer zones, float and flowtop or basal breccias returned weakly to moderately anomalous values in mercury. Seven soil samples also returned isolated moderately anomalous values in mercury. Samples anomalous in mercury were not found to be anomalous in other metals.
14
Maps showing the location of geochemical samples and geology are in the pocket at the end of this report. These maps
have been prepared from base maps supplied by McMillan Bloedel Limited at a scale of 1:5,000.
15
ACKNOWLEDGEMENTS
The writer gratefully acknowledges guidance from C. J. Hickson while mapping in the field and for fruitful discussions during the writing of this report.
16
REFERENCES
1. Hickson, C.J., 1988, Structure and StratiaraDhY of the Masset Formation Oueen Charlotte Islands British Columbia in Current Research G.S.C. Paper 88-1E pp 269-274.
2. Hickson, C.J., 1989, Structure and Stratiarawhy of the Masset Formation Oueen Charlotte Islands British Columbia in Current Research G.S.C. Paper 89-113 in press.
3 . Sutherland Brown, A . , Geoloqv of the Oueen Charlotte Islands: British Columbia Department of Mines and Petroleum Resources Bulletin 54. p 226.
STATEMENT OF QUALIFICATIONS
I, MICHAEL P. TWYMAN, residing at 4687 Tourney Road, North Vancouver do hereby testify that
1. I am a practicing Geologist and have been since 1984 after completing a Bachelor of Science in Geology at the
University of British Columbia.
2. I am a Fellow of the Geological Association of Canada.
3 . The conclusions and statements in this report are the
result of my observations made in the field.
Vancouver, British Columbia
November, 1988
APPENDIX 1
ANALYTICAL DATA
ro . Cl'I'k' l<ESOllRCES ( C A N A I ) A ) LIMITED
Chemex Analytical Chemlsts * Geochemlsts Labs Reglstered Ltd. AJsayers 2000 - 666 B U R R A R D ST.
V 6 C 2x8 2 1 2 BROOKSBANK AVE. . NORTH VANCOUVER, VANCOUVER, B C BRITISH COLUvlBIA, CANADA V7J-2CI
PHONE ( 6 0 4 ) 9 6 4 - 0 2 2 I C o r n m e n I s : ATTN: JOHN DEIGHTON CC: MICHAEL 'IUIYMAN
A881846 6
CITY RESOURCES (CANADA) LIMITED PROJECT :LINDA B E A N
I
j CODE NlWtl3ER
SMJ'LES DESCRIPTION METHOD DETECT t ON UPPER LIMIT L I M I 7
S a m p l e r r u b m i t t e d t o our lab in V a n c o u v e r , BC. T h i r r e p o r t wao p r i n t e d on 15-JUL-88.
I SAMPLE PREPARATION I DESCRIPTION
NOTE 1 :
T h e 32 element ICP, p a c k a s e i t r u i t a b l e for t r a c o metal, in foil a n d r o c k s a m p l e s . E I e m e n t t for w h i c h t h e n i t r i c - a q u a r e g i a d i g e s t i o n i r p o r e i b l y i n c o m p l e t e a r e : A I , Ba, Be, C a , C r , Ga. K, L a , M g , N a , Sr. Ti, T1, W.
1 0 0 2 3 4 5 6 7
1 3 1 6 20 2 2 2 3
!
4 4 4
l 4
A u ppb: Fuse 10 g sample Cu ppm: HN03-aqua regia digest M o ppm: HNOI-aqua regia discst P b ppm: HNOI-aqua regia di8est Z n ppm: HN03-aqua redfa di8e6t Ag ppm: liN03-aqua regia digest Cd ppm: HNO3-aqua re8ia d i~eo t Ac ppm: HN03-aqua rosia disert Se ppm: HCI-KC103 digest, ext Hs ppb: HN03-HCI digestion
Sb ppm: HCI-KC103 digest, extrac Bi ppm: HCI-KC103 digest, extrac
FA-AAS AAS '
AAS-BKGD CORR AAS AAS-BKGD CORR AAS-BKGD CORR AAS-HYDRIDE/EDL AAS-BKGD CORR AAS-FLAMELESS AAS-BKGD CORR AAS-BKGD CORR
5 1 1 I 1
0 . 2 0 . I
1 0 . 2 10
2 0 0 200
TO : CITY RESOURCES (CANADA ) LIMITED
Chemex Labs Ltd. P a g e No. : 1 Tot. Pages: 1
Invoice : 1-8818466 P . O . :NONE
Date : 15-JUL-88 2000 - 666 BURRARD ST. VANCOUVER, BC V6C 2x8
- - - Analytlcal Chemlsts * Geochemists Reglstered Assayers
2 I 2 BROOKSBANK A V E . . NORTH V A N C O U V E R , BRITISH COLLMBIA. CANADA V7f-ZC;I
PHONE ( 6 0 4 ) 9 8 4 - 0 2 2 1
P r o j e c t : L I N D A B E A N Conmenis: A T T N : JOHN D E I G H T O N CC: MICHAEL 'IWYUlrN
I CERTIFICATE OF ANALYSIS A8 8 1 8 4 6 6 1 SAMPLE
DESCRIPTIOF PREE CODE
Pb P P
Cd P W
H g PPb
23: 23: 2 3: 2 3!
0 . 0 . 0. 0 .
C 8 8 W 11 C88IMiH 19 C88IMiH 31 C88IMXH 68
I < 5 ; < 5
2 21 I
0.1 0.1 0 . 1 0.1 0 . 1
0.2 0.2
- - -
Chemex Labs Ltd. Tot. Padel: 1 Date : 13-JUL-88 2000 - 6 6 6 B U R R A M ) ST.
VANCOUVER, BC Invoice II : 1-88 16468 V6C 2x8 P.O. I :"E
ProJeci : L I N D A - D U N C o m n i s : ATTN: JOHN DEICHTON CC: MICHAEL IW%&+N
Analytlcd Chomlets Goochomlrts * Roglstored Assayer s 2 I 2 BROOKSBANK A v E . . NORTH VANCT)UVER. BRITISH COLIMBIA. UNAUA v7.r-ICI
PHONE ( 6 0 4 ) 9 8 4 - 0 2 2 1
CERTIFICATE OF ANALYSIS A8 8 1 8 4 6 8 1 SAMPLE
DESCRIPTION
a P p n
zn P p n
0. I 0.1 0.3 0 . 1 0 .2
0. I 0. I 0. I 0.2 0.1
0. I 0.1 0.1 0.1 0. I
0.1 0.4 0.7 0.1 0.1
0.7 0.5 0.2 0.1 0.1
0.1 0 . 1 0 . 1 0 . 1 0 .1
0 .1 0 . 1
5 8 76 114 57 150
34 28 74
129 2 1
76 32 49 26 34
1 7 3 6 5 64 26 54
3 8 3 3 40 26 2 7
63 71
0. I 0. I 0. I 0. I 0. I
0 . 1 0 . 1 0 . 1 0 . 1 0 .1
0. I 0 . 1 0.1 0. I 0. I
0. I 0.1 0 . 1 0.1 0.1
0. I 0.1 0.1 0 .1 0 .1
0.1 0 . 1
7 12 23
1 2 4 5
0.2 0.2 0.2 0 . 2 0.2
0.2 0.2 0.2 0.2 0.2
--
---
0.2 0.1 - C88LMlRO7 C88LMIRlO C88LMIR14 cB8LMIR16 cB8-18
40 180 2600 5700 130 0 . 2 1 O . i ( 50 40 30 30 20
C88-3 c88-7
0 . 2 0 . 1
6.0 0.1 1 .o 0.1
3 30 0.6 0.1
510 1 1 . 0 0.1 520 5.4 0.1
0.2 3 40 1.6 0.1 0 . 2 280 0 . 8 0 .1 0 . 2 4 9 0 0 . 4 0 .1 - -q 0 .2
< 5 . 5 < 5 ! 5 < 5 : 5 < 5 ; 4
I/ 6 5
1
CERTIFICATE OF ANALYSIS A8 8 199 1 1 1
1 7 4 . 0 .1 3 5 i 0.1 2 5 : 0 .1
5 4 ' 0.1 1 2 5 ' 0 . I
8 9 ' 0 . I b6 0 . I
1 2 1 0 . I
- - -.. --! .--
L
17 0.2 330 0.4 0 .1 6 0 . 2 30 0 .1 0 .1 7 0 . 2 0 . 2 6 . 1
0 .1 0.1
I ; I ! I
I CBRTIFICATE OF ANALYSIS A8 8 19 9 58
20 0.32 I21 7 4 . 6 4 10 < I 0.01 20 0.14 821
25 7 . 2 4 < 10 < I 0 . 0 2 30 0.47 13X 20 3 . 0 0 < 10 < 1 0.04 20 O.?3 637 2 5 3 , 5 3 < 10 1 3 0.m 30 1 . W 644
22 4 . 5 5 < 10 < 1 0.04 20 6-70 721 a 2.30 < lo I 0.04 2 0 0.37 397
I 1 J . 1 3 <: LO 1 0.01 20 0.54 3f : I 5 3.90 c 10 < 1 0.06 70 0.s9 52(
7 71 2 0 f.97 < 1 0 < I O.# 2 3s
< S 1.18 0 . 4 < 5 1 6 0 0.5 t 42 t 4 7 C 5 1.11 ( 0 . 1 < 5 2JO Q . 5 C I 1.10 U.5
49 6 3 4
C 5 1.49 0 . 4 < J 90 ( 0 . 5 C I 0.66 < O . S < 5 1 . 4 a c0.z < 5 7 0 C O . 5 < 1 0 . 6 1 < 0 . 1 5 2:
LO 1 . 2 1 0 . 2 < s 54) c o . 5 < 2 0 . 4 & < 0 > LO t 35 60 c o . 5 < 1 0.)1 € 0 . 1 LO 1 . 5 0 < 0 . 2
1 6 0 1.72 0.2 < 5 40 c o . 5 i 0.1) c 0 . 5 < s 0.62 0 . 2 < 5 50 ca.5 < 3 0 . 1 s < 0 . 5
< S 1 - 3 4 ( 0 . 1 < 5 10 cu.5 < 1 0 . 8 5 <U.$ 2 0.7a 0 . 5 17 a5
I-------- .. . -
DBSOlIPTJOOlr
(uc L l O l U a C L102 (Ipc tl04
Aapgb A l 4 d Ba B. Bi Ca Cd Co Cr QI Fe G. 4 r t r y L a 9 s ~ p p P p c m ~ p p n % p g m p p a O Q n a p g m s b m o p n % g p o s p a
< 3 3.16 0.6 )o <o.s < 2 0.02 0 . 1 I 34 28 30.31 10 I 0-0s w 0.01 618 20 0.12 241 < 5 3 . M 0.6 15 20 < O . l < 2 0.03 < O . 5 2 x) 13 7.04 20 < 1 0.03
< 3 4.14 ( 0 - 2 < 5 20 < O . I < 2 0.01 < 0 . 1 < I 13 s s.3a m < 1 0-02 20 0 . 0 3 loc 10 < 1 0-02 20 0.11 lo1 < 9 7.64 0 . 4 < 5 3 0 < o . 1 < 2 0.02 0.5 J 26 7 s.24
--
201 238 t O J 238
201 231 201 ,238 101 23t
201 238
201 238 201 238 201 238 201 238 201 238
201 238 201 234 201 238 201 238 201 238
mi 23a
mi 23a
201 ;238 201 1211
I
. < 5 2 . t6 0 . 2 2 0 40 0 . j 2 0.01 < 0 . ) < I 1 2 3 5 . 2 9 10 < I 0.20 30 0.03 4a 20 0.13 IS?, < 5 1.03 0.4 2 0 )c) 0.5 4 2 0.02 < 0 . 1 4 24 8 5.m 10 < I 0.03
c I t . 1 2 ( 0 . 2 5 10 < 0 . 5 4 < 0.01 < o . s < 1 8 2 2 . t 2 10 < I 0.02 M 0.01 72' < 5 3.24 0 . 2 5 to C O . 5 2 0.02 < 0.5 16 J 1 27 7.61 < 10 < I 0.02 10 0.12 4S9
C 5 7.27 0.4 < 5 4 0 0 . 1 2 0.02 0.1 2 1 45 21 9.17 10 < I 0.02 2 0 0.34 L24 < 5 2.14 <Q.2 J 20 c 0 . i < 2 0.01 c 0 . 1 I 17 9 5 . 2 0 2 0 < I 0.02 )o 0.04 a4 c 5 1 . 1 2 0.4 2 s 10 1.0 < 2 0.03 < 0.3 6 I6 10 4.18 LO < I 0.04 2 0 0 . 1 2 242 < J 0 .81 ( 0 . 2 10 10 < 0 . 1 < 2 < 0.01 c 0 . 5 I 6 2 2 . 9 0 1 0 < ! 0.02 )o 0.01 17b < 5 5 - 8 5 0 . 2 c 5 $0 0 . 1 c 2 0.01 < 0 .1 S 11 11 4.79 LO < 1 0.0s 20 0.16 tbP
-I__-- -_1__1_
Chemex Labs Ltd
c s 1.06 (0.2 10 150 0 . 5 < 2 0.26 < 0 . j 4 1 5 11 3.79 < LO C 1 0 . 1 3 w) 0.22 1800 x) 0 . 8 % 116s c 5 4.70 ~ o . 2 < 5 iao 1 . I 4 2 0.47 0 . 5 22 24 24 6 . 1 1 LO
< , 5 3.a <0.1 c 5 130 0 . ) c 2 0 . 9 5 c 0.1 36 17 17 4 . 5 5 10 < 1 0.08 3 4 0.- 1180 < 5 2 . W C Q . 2 < 5 260 0 . ) < 2 0 . 7 5 < 0.1 21 1 3 5 4.38 to < 1 0-06 K) 0.26 HOOOOl
c J 3 . 1 a 4 0 . 2 c 5 1 2 0 0 . 1 c 1 0 . a 7 < O . J I6 17 17 4.63 10 < 1 0-0) 20 0.79 3225 < I 2.79 < Q . 2 < 5 SO 0 . 5 4 1 0 . 9 6 < 0 . 1 1 7 32 2a 4 9 8 10 < 1 0.03 #) 0.J6 ISM < 5 1.77 ( 0 . 2 < 5 8 0 0 . 3 < Z 0 . M C 0.5 I2 A 4 3.49 < 10 < 1 0.07 20 0.2a m o c J 2.13 e 0 . 2 < s IX) 1 . 0 4 2 0 . a 2 < 0 . 5 I 1 14 19 3 , 5 8 < 10 C 1 0,- 3 4 0.70 1395 C 3 3.23 ( 0 . 2 4 5 1 4 0 0 . 5 < 2 0 . 9 6 C 0.5 19 45s 37 4 .20 1 0 c 1 0.08 30 1 . 4 0 1135
1 0 .11
-- ------
- C I 3.51 ( 0 . 2 < 5 I 3 0 I . O C 2 0.92 < 0.5 2 0 31 2a 4 , u < JO c I 0.07 )o 1 . 0 5 1l40
)o 0.78 1 4 0 5 c 5 3.a7 ( 0 . 2 < 5 140 0 . 5 < 2 1.00 0.3 I f 32 16 3 . 9 2 < 10 < 1 0.06 < 5 3 . 1 1 ( 0 . 2 < 5 I30 0 . 1 < 2 0 . 6 3 0.5 16 16 16 3 . 9 4 < 10 C 1 0.06 20 0.71 102s C I 2 . 6 0 0 . 2 I5 90 0 . 1 < 2 0 . 6 4 C 0.1 1 3 11 19 4.01 10 < 1 0.09 20 0.70 1245
IbQTlBD
0 . 1 0 . 1 0 . 1 0 . 1 0.1
2 1 1 1 2
0 . 2 0.2 0 . 2 0 . 2 0 . 2
TO : C I'N RESOUICES (CANADA ) L IMITED P;\(lC NO. : I Tot. PagCS:2 D A t C : I 5-JUL-hb Invoice # : 1-88 18467
2000 - G G G BUIIRARD ST, VANCOUVER, BC VGC 2x8 P . O . ff :NONE
P r o j e c t : L I N D A - U E A N Comments: A T T N : JOHN U E I C H T O N CC: MICHAEL IWYMAN
Chernex Labs Ltd. Analytlcal Chomlsts Geochemlsts Reglstered Assayer s
2 1 2 BROOKSBANK AVE . NORTH V A N C O l l V E R . BRITISH COLClMUIA, CANADA V7J-ZCI
PHONE ( 4 1 ) 4 ) 9 8 4 - 0 1 2 1
I CERTIFICATE OF ANALYSIS A8 8 1 8 4 6 7 1 I
iu ppb .Cu =A+M 'ppn
!
< 5 ' 7 < 5, 10 < 5 , 20 < 5 2 7 < 5 ; 42
SAMPLE PREP DESCRIPTION I CODE
I
Zn P P
4s Ag PPn Aqua R P P
1 I 10 3
1 23 I
2 0 1 I -- 2 0 1 1 - 2 0 1 -- 2 0 1 -- 2 0 1 -
65 107 93 82 73 53 70 8 8 94 93
75 77 70 93 58
95 65 28 121 50
32 46 59 62 45
38 43 19 10 28
55 36 40 20 115
112 76 90 19 40
- --
---
..- . . -
. _--
- _.- ._-
. . . - -- -
- _-.._ --
0. I 0.3 0.2 0.1 0.1
--
0.1 0.1 0.1 0.1 0.1
0.1 0.1 0.1 0.1 0.1
0. I 0.1 0.1 0.1 0.1
---
--
- --. ..- -.
190 1 6 0 2 1 0 6 1 0 1900
8 1 0 2000
1 8 0 140 150 150 3 40
3 90 3 40
0.2 0 . 1 0 . 1 0 . 2 0.1
0 . 1 0 . 1 0 . 2 0 . 1 0 . 1
0 . 2 0 . 1 2 . 6 0 . 2 0 . 1
1 . 4 1 .o 0.2 1.4 0.8
2 . 6 1 . o 0.2 0.1 0 . 1
0 . 4 1 .o 8 . 0 2 . 6 0.4
0.4 0.8 1.2 0.4 0.1
---
-. -..--
--
- --
--.-
--
7
6 5
-110.2 2 0 1 I -
-- 2 0 1 - 2 0 1 - 201 -- 2 0 1 -- 2 0 1 - 2 0 1 - 2 0 1 ' --
- $ 1 - --
2 0 1 - 2 0 1 ' - 2 0 1 I - 2 0 1 ' - 2 0 1 1 --
1 1 1 4 1 1 1 2 1 4
0 . 2 0.2 0.2 0.2
0 . 2 0.2
1 0.2 0.2
0.3 0.1 0.2 0.5 0.2
0.1 0.1 0.1 0.3 0.2
0.1 0.2 0.2 0.1 0.2
0.1 0.1 0.1 0.1 0 . 2
-^-_ _-_
--_-
.---.--
---
2 1
0 .1 0 . 1 0. I 0 . 1 0. I
0.1 0.1 0.1 0.1 0.1
0.1 0. I 0.1 0.1 0. I
.- ---
--_-
-.--
410 530
6 70
90 0.2 5 70 500 2 20 890 6 30
1 8 0 0 0 . 2 860
0.2 420
_- -- a a n 4 9 a m n s o amn5i a m n s 2 a m 4 . n 5 3
2 0 1 I -
2 0 1 I -- 2 0 1 i - 2 0 1 I - 2 0 1 j -- :I 6 !;;I
a w n s 4 a a u n s s a w n s 6 a w n 5 7 c8aWTLS8
201 ! - 2 0 1 , - 2 0 1 I - 2 0 1 1 - 2 0 1 ; - 1 8
1 1 1 1 7 1 4 1 4
2 0 1 : - 2 0 1 I - 201 i - 2 0 1 - 2 0 1 1 - 3 5 0
0 . 2 3 90 230 1 4 0
4 1 I I
C E R T l F l C A T l O N :
As PPn
6 17 3 3 7
! Se i Sb 1 B i P P PPb 'Ppn ppn
14 0.
0.2 0. 0 . 2 17( , 0.4 0.2 69 ! 0.8 0.
--.---
-. 0.2 101 0.2 13( 0.2 220i 0.2 184 0.2 54(
0.2 3 2( 0.2 2 4( 0.2 3 5( 0.2 15( 0 . 2 1 2 3 I----
.. - I .- A
'ai Lj ,& 1, \ 3 u L .i I..
Page No. . 2 Tot. P a g e s 1 2
Invoice (I : 1 - 8 8 ] 8 4 6 7 Date : 1 S-JUL-bb
P.O. i :"E
TO : CITY RESOURCES ( CANADA 1 L IMITED
Chemex Labs Ltd. 2000 - 666 BURRmD ST. VANCOUVER, BC V6C 2x8
ProJtcl : LINDA-DEAN Cornnenis: ATTN: JOHN DEIGHTON CC: MICHAEL "%IAN
~ . - - - AnalytlOal Chomlsts * Geochemists * Replstered Assayer J
2 I 2 BROOKSBANK A V E . , NORTH VANCOlWER. B R I T I S H C O L W I A , CANADA V7.1-2CI
PHONE ( 6 ( 1 4 ) 9 6 4 - 0 2 3 1
CERTIFICATE OF ANALYSIS A8 8 1 8 4 6 7 I ,
PREF CODE
Pb P p n
Pprn
201 201 201 201 201
201 201 201 201 201
-
-
..--
---
0.2 0 . -
-- -
.. . .--_.
--..--.-.
..-. . ...-..-- .- ..--__. - !
STATEMENT OF COSTS
Room and Board 34 days Q $ 55/day
T r u c k Rental 34 days Q $ 50/day + gas
A i r Fare Airfare Vcr-Sandspit return
Ass?.-- Costs
Report Preparation (writing, map preparation, drafting) 7 days @ $225/day
Office C o s t s
Total expenditure
" R28
Grab sample of weakly silicious rhyolite breccia, trace pyrite and minor iron oxide staining.
A s above,
Select grab from rhyolite breccia.
Grab sample of rhyolite tuff with thin chloritic bands crosscut by rhyolite breccia stringers. Minor disseminated pyrite.
Chip sample across 1 m wide shear in rhyolite tuffs and flow breccias. Strong oxidation in sheer zone,
Chip sample in rhyolite tuff minor oxidation and trace amounts of pyrite.
Chip across 1.5 m of rhyolite breccia.
Grab from silicious fine grained intrusive (andesite?) 1% finely disseminated magnetite -5% disseminated pyrite.
Grab from rhyolitic flow breccia, trace of pyrite, hematitic staining common.
Chip across 5 m brecciated silicified flow banded rhyolite? Abundant iron-oxide staining.
Random chip across intensely silicified rhyolite flow breccia, Abundant iron oxide staining on fractures,
Volcanic breccia similar in appearance to R16 and R22 minor pyrite strong iron staining.
Chip across 5 m of variable light grey to pinkish to dark grey rock. Pervasive silicification andesitic? Rhyolitic flow?
Grab sample from felsic breccia fragments up to 30 cm. Heavy iron oxide staining, minor hydrothermal alteration.
Chip sample across 5 m of brecciated volcanic tuff .
Description of Rock Samples continued:
C88LMTR33 Select chip from strongly iron stained and brecciated andesite?
I' R37 Grab from rusty pinkish flow-banded rhyolite.
'I R40 Grab sample as above.
'I R46 Select chip from "cherty" rhyolite with .5 mm quartz stringers contianing minor pyrite and rare marcasite.
R60 Grab from whitish grey rhyolite tuff breccia. Abundant calcite stringers 1-2% pyrite and rare chalcopyrite in narrow ( - 5 mm) stringers.
I' R61
'I R63
'I R70
Select grab from rhyolitic breccia containing up to 50% pyrite as irregular blebs.
Random chip across brecciated flow banded rhyolite. Weak argillic alteration.
Random grab from flow-banded rhyolite with abundant 1-2 mm stringers of pyrite.
Grab from f low-banded tuff with 1-2% disseminated arsenopyrite and lesser pyrite.
Select grab sample of rhyolitic breccia with moderate argillic alteration. Up to 50% fine grained pyrite and arsenopyrite.
'I R71 Chip across 2 m wide fault crosscutting rhyolitic flows.
'I R73 Select grab from float. Dacitic flow-banded tuff up to 2% disseminated pyrite.
(* R75 Grab sample from strongly clay altered flow- banded rhyolite locally brecciated along fractures. Brecciated zones infilled with 1-5 mm quartz stringers containing traces of fine grained pyrite and arsenopyrite,
I' R76
'I R79
Silicified flow-banded rhyolite with 1-2 mm pyritic vugs. Float sample.
Description of Rock Samples continued:
C88LMTR80 Silicified flow-banded rholite up to 50% pyrite in fine grained masses from float.
" R86 Select chip across 3 m wide fault zone in flow- banded rhyolites. Up to 50% pyrite in fault gouge.
'I R87
" R89
Select grab from dark grey flow-banded rhyolite with up to 50% disseminated pyrite.
Chip sample across 1.5 m fault bounded contact between basaltic lahar and silicified brecciated rhyolite.
" R91 Select grab from light grey fine grained andesite with up to .5% disseminated pyrite.
" R93 Random grab from silicified lapilli tuff with trace disseminated pyrite.
" R99 Random grab of a locally brecciated flow-banded rhyolite with weak argillic alteration.
"R109 Grab sample from argillicly altered rhyolite with 2-3% pyrite.
"R110 A s above.
"R113 Random chip across 1 m of brecciated rhyolite flow containing minor disseminated 5 mm clumps of pyrite.
"R114 Chip across andesite dyke with 2-3% disseminated pyrite and numerous narrow quartz stringers containing minor pyrite.
"R115 Select chip/grab sample from pyritic rhyolite flow.
"R121 Grab sample from rhyolite breccia.
"R124 Grab sample from rhyolite breccia with up to 10-15% disseminated pyrite.
"R125 Random grab from sulphide rich gouge and strongly clay altered rhyolite. up to 20% sulphides.
Description of Rock Samples continued:
C88LMTR126 Random grab from locally flow-banded rhyolite with weak argillic alteration containing minor pyrite.
I' R131
It R134
Grab sample from weakly pyritized (.5-1%) brecciated rhyolite.
Select grab of a silicious feldspar quartz porphyry with 5% disseminated pyrite.
Select grab of a silicious feldspar quartz porphyry with 5% disseminated pyrite,
Grab sample of a silicified felsic rock aphanitic, aphyric with 5% disseminated pyrite.
Grab sample as above with 10% disseminated pyrite.
Select grab from a fractured strongly clay- altered dacitic flow.
Chip-grab sample from a 1.5 m wide shear zone.
Chiphelect grab samples over 4 m of quartz vein stockworking in felsic flow rocks. 5% sulphides, pyrite and lesser arsenopyrite.
I' R158 ( 2 - 4 m)
As above.
SCALE 1:5000
LINDA-BEAN CLAIMS
GEOLOGY AND
SAMPLE LOCATION
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LEQENO 3 /
LINDA-BEAN CLAIMS
GEOLOGY AND
SAMPLE LOCATION
B I R D
L A K E
LINDA-BEAN CLAIMS
GEOLOGY AND
SAMPLE LOCATION
C
b- .
SCALE 1:5000